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231225s2016 xx |||||o 00| ||eng c |
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|a 10.1002/2015JD024267
|2 doi
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|a pubmed25n1046.xml
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|a DE-627
|b ger
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|e rakwb
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| 041 |
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|a eng
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| 100 |
1 |
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|a Tao, Wei-Kuo
|e verfasserin
|4 aut
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| 245 |
1 |
4 |
|a The relationship between latent heating, vertical velocity, and precipitation processes
|b The impact of aerosols on precipitation in organized deep convective systems
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|c 2016
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
|b c
|2 rdamedia
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|a ƒa Online-Ressource
|b cr
|2 rdacarrier
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|a Date Revised 10.01.2021
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|a published: Print-Electronic
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|a Citation Status PubMed-not-MEDLINE
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|a A high-resolution, two-dimensional cloud-resolving model with spectral-bin microphysics is used to study the impact of aerosols on precipitation processes in both a tropical oceanic and a midlatitude continental squall line with regard to three processes: latent heating (LH), cold pool dynamics and ice microphysics. Evaporative cooling in the lower troposphere is found to enhance rainfall in low cloud condensation nuclei (CCN) concentration scenarios in the developing stages of a midlatitude convective precipitation system. In contrast, the tropical case produced more rainfall under high CCN concentrations. Both cold pools and low-level convergence are stronger for those configurations having enhanced rainfall. Nevertheless, latent heat release is stronger (especially after initial precipitation) in the scenarios having more rainfall in both the tropical and midlatitude environment. Sensitivity tests are performed to examine the impact of ice and evaporative cooling on the relationship between aerosols, LH and precipitation processes. The results show that evaporative cooling is important for cold pool strength and rain enhancement in both cases. However, ice microphysics play a larger role in the midlatitude case compared to the tropical. Detailed analysis of the vertical velocity governing equation shows that temperature buoyancy can enhance updrafts/downdrafts in the middle/lower troposphere in the convective core region; however, the vertical pressure gradient force (PGF) is the same order and acts in the opposite direction. Water loading is small but on the same order as the net PGF-temperature buoyancy forcing. The balance among these terms determines the intensity of convection
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|a Journal Article
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|a CCN
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| 650 |
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|a aerosol
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| 650 |
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|a cold pool
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| 650 |
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4 |
|a convection
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| 650 |
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|a latent heat
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| 650 |
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4 |
|a precipitation
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| 700 |
1 |
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|a Li, Xiaowen
|e verfasserin
|4 aut
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| 773 |
0 |
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|i Enthalten in
|t Journal of geophysical research. Atmospheres : JGR
|d 1998
|g 121(2016), 11 vom: 16. Juni, Seite 6299-6320
|w (DE-627)NLM098183494
|x 2169-897X
|7 nnas
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| 773 |
1 |
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|g volume:121
|g year:2016
|g number:11
|g day:16
|g month:06
|g pages:6299-6320
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| 856 |
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|u http://dx.doi.org/10.1002/2015JD024267
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